RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 10, ES3002, doi:10.2205/2007ES000233, 2008

Figure 9. Stream function of zonally averaged meridional circulation and its response in the
Atlantic Ocean (a) and the Pacific plus Indian oceans (b). The solid contours denote the positive
values of the meridional stream function, which correspond to the clockwise motion, and the
dashed contours denote the negative values, corresponding to the counterclockwise motion. The
response of meridional circulation to increased CO2 is shown with the aid of shading with the
gradation scale on the right.

Citation: Diansky, N. A., and E. M. Volodin (2008), Study of the ocean response to climate changes in XX–XXII centuries, simulated with the coupled atmosphere-ocean general circulation model, Russ. J. Earth Sci., 10, ES3002, doi:10.2205/2007ES000233.
Copyright 2008 by the Russian Journal of Earth Sciences
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